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首页> 外文期刊>Solid state sciences >Properties of the perovskites, SrMn_(1-x)Fe_xO_(3-#delta#) (x = 1/3, 1/2, 2/3)
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Properties of the perovskites, SrMn_(1-x)Fe_xO_(3-#delta#) (x = 1/3, 1/2, 2/3)

机译:钙钛矿的性质SrMn_(1-x)Fe_xO_(3-#delta#)(x = 1 / 3、1 / 2、2 / 3)

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The SrMn_(1-x)Fe_xO_(3-#delta#) (x = 1/3, 1/2, 2/3) phases have been prepared and are shown by powder X-ray and neutron (for x = 1/2) diffraction to adopt an ideal cubic perovskite structure with a disordered distribution of transition-metal cations over the six-coordinate B-site. Due to synthesis in air, the phases are oxygen deficient and formally contain both Fe~(3+) and Fe~(4+). Magnetic susceptibility data show an antiferromagnetic transition at 180 and 140 K for x = 1/3 and 1/2, respectively and a spin-glass transition at 5, 25, 45 K for x = 1/3, 1/2 and 2/3, respectively. The magnetic properties are explained in terms of super-exchange interactions between Mn~(4+), Fe~((4+#delta#)+) and Fe~((3+#epsilon#)+). The XAS results for the Mn-sites in these compounds indicate small Mn-valence changes, however, the Mn-pre-edge spectra indicate increased localization of the Mn-e_g orbitals with Fe substitution. The Mossbauer results show the distinct two-site Fe~(3 + #epsilon#) + /Fe~((4 + #delta#) +) disproportionation in the Mn- substituted materials with strong covalency effects at both sites. This disproportionation is a very concrete reflection of a localization of the Fe-d states due to the Mn-substitution.
机译:已经制备了SrMn_(1-x)Fe_xO_(3-#delta#)(x = 1 / 3、1 / 2、2 / 3)相,并用粉末X射线和中子表示(对于x = 1 / 2)衍射以采用理想的立方钙钛矿结构,过渡金属阳离子在六坐标B位上无序分布。由于在空气中的合成,这些相缺氧,并且形式上同时含有Fe〜(3+)和Fe〜(4+)。磁化率数据显示x = 1/3和1/2分别在180和140 K处发生反铁磁转变,x = 1 / 3、1 / 2和2 /分别在5、25、45 K处发生自旋玻璃转变3,分别。用Mn〜(4 +),Fe〜((4 +#delta#)+)和Fe〜((3 + epsilon#)+)之间的超交换相互作用来解释磁性。这些化合物中Mn位点的XAS结果表明Mn价态变化很小,但是Mn前缘光谱表明Mn-e_g轨道被Fe取代的位置增加了。 Mossbauer结果表明,在Mn取代的材料中,Fe〜(3 +#ε#)+ / Fe〜((4 +#delta#)+)的分布明显不同,这两个位点均具有很强的共价效应。这种歧化是由于Mn取代而引起的Fe-d态局部化的非常具体的反映。

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